ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
华北陆块南缘金矿成矿动力学探讨
  
关键词:North China plate  late period of orogeny  granite  gold deposit  thermal hydraulic metallogenic model
基金项目:中国地质调查局国土资源大调查项目(编号:200110200038)
作者单位E-mail
朱嘉伟 河南农业大学资源与环境学院河南郑州450002 zhujw686@163.com 
赵盼舒 南京邮电大学江苏南京210033  
李锋 夏邑县国土资源局河南夏邑476400  
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摘要:
A Discussion on Mineralizaion Dynamics Mechanism of Gold Deposits on the Southern Edge of the North China Plate
      Unstable isotope analyses show that there is no relationship between gold deposits and granite in Xiaoqinling-Xiongershan area.This paper has studied the age and space relationship between the gold deposits and the granite as well as the formation dynamics of the gold deposits.The authors consider that it was the evolution of the Yanshanian granitic magma that caused the formation of the gold deposits.The ore elements-bearing fluids formed and evolved with the whole process of the granitic magma evolution.In this process,the granitic magma not only offered ore-bearing elements but also huge thermodynamic energy for mineralization.The Yanshanian detachment tectonic belt performed as the main regional ore-controlling and ore-hosting structure.A gold mineralization model,i.e.the Magmatic Thermodynamic Gold Mineralization Dynamics Mechanism is given in this paper,which is of great significance in gold deposit exploration.
ZHU Jia-wei,ZHAO Pan-shu,LI Feng.2008.A Discussion on Mineralizaion Dynamics Mechanism of Gold Deposits on the Southern Edge of the North China Plate[J].Acta Geoscientica Sinica,29(4):525-532.
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